SOIL MAPOF PLATANOULIA SCALE 1:20,000

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1 SOIL MAPOF PLATANOULIA SCALE 1:20,000,^y^~^-^ z^ Sf^^^Jy^ J /f f f ^4-^ Kalamakiouv tî narrows N^ ft V ^^V s^n^s>\ j n i\ f^! ' Jzx>C^ U afe V^y^ç :Paved roads Rivers Unpaved roads all weather dry weather Stream/ SSEIL^C- '10- Contour fo Soil profile ~ Soil section ryh n u (soil physicaland/or chi ' ' ' 3 data supplied in this

2 LEGEND N 1. SOILS OF THE PLEISTOCENE TERRACE a. higher level DEEP, WELL DRAINED SOILS HAVING A LOAMY SURFACE OVER A THICK CLAYLOAMY Bt HORIZON DEEP, MODERATELY WELL DRAINED SOILS HAVING A LOAMY SURFACE OVER A VERY THICK, CLAYLOAMY Bt HORIZON DEEP, WELL DRAINED SOILS HAVING A LOAMY SURFACE OVER A THICK, CLAYEY Bt HORIZON DEEP, MODERATELY WELL DRAINED SOILS HAVING A LOAMY SURFACE OVER A THICK, CLAYEY Bt HORIZON MODERATELY DEEP, WELL DRAINED, CLAYLOAM SOILS HAVING AN ARGILLIC HORIZON MODERATELY DEEP, WELL DRAINED, CLAY SOILS HAVING AN ARGILLIC HORIZON MODERATELY DEEP, MODERATELY WELL DRAINED, CLAY SOILS HAVING AN ARGILLIC HORIZON DEEP, WELL TO MODERATELY WELL DRAINED, CRACKING CLAY SOILS HAVING AN ARGILLIC HORIZON DEEP, MODERATELY WELL TO IMPERFECTLY DRAINED, CRACKING CLAY SOILS HAVING AN ARGILLIC HORIZON SHALLOW, WELL TO EXCESSIVELY DRAINED, FINE TEXTURED SOILS HAVING A SHALLOW CAL \t HORIZON b. middle level DEEP, WELL DRAINED, CLAYLOAM SOILS HAVING AN ARGILLIC HORIZON DEEP, WELL DRAINED, MEDIUM TEXTURED SOILS HAVING A CAMBIC HORIZON 2. SOILS OF THE HOLOCENE TERRACES DEEP, WELL DRAINED, CLAYLOAM SOILS HAVING AN ARGILLIC HORIZON MODERATELY DEEP, WELL DRAINED, MODERATELY FINE TEXTURED SOILS HAVING A CALCIC HORIZON 3. SOILS OF THE FLOOD PLAIN MODERATELY DEEP, EXCESSIVELY DRAINED, CALCAREOUS, COARSE TEXTURED SOILS MODERATELY DEEP, WELL DRAINED, CALCAREOUS, MEDIUM TEXTURED SOILS MODERATELY DEEP, WELL DRAINED, CALCAREOUS, MODERATELY FINE TEXTURED SOILS :hemical is study) Man made hills Bonder of the study area km

3 SCALE 1:25,000 PI Soil profile T3 Soil section (chemical dataavailable) Soil section (data on CEC, ESP, ECe) Contour Rivers.,.-- Streams Paved roads "V Unpaved roads - ftvft Urbar

4 En twf um mm LEGEND N SOILS OF THE BEACH RIDGES BREpxl VERY COARSE TEXTURED, EXCESSIVELY DRAINED SOILS BREpx2 COARSE TEXTURED, EXCESSIVELY DRAINED SOILS SOILS OF THE CHANNEL BELT (Nearly flat, very stratified, calcareous,alluvial soils with fluvic properties) AcExl AcEx2 SANDY LOAMY SOILS, SOMEWHAT EXCESSIVELY DRAINED MEDIUM OVER COARSE TEXTURED, WELL DRAINED SOILS SOILS OF THE MEANDERING BELT AmExl AmEx2 (Nearly flat, deep, stratified, calcareous, alluvial soils with fluvic properties) COARSE OVER MEDIUM TEXTURED, WELL DRAINED SOILS MEDIUM TOMODERATELY FINE LMR COARSE TEXTURED SOILS, WELL TO MODERATELY WELL DRAINED AmEx3 MODERATELY FINE TEXTURED SOILS, WELL TO MODERATELY WELL DRAINED AmExa COARSE TO MEDIUM TEXTURED SOILS, MODERATELY WELL DRAINED / AmEae MEDIUM TEXTURED, POORLY DRAINED SOILS SOILS OF THE BACKSWAMPS Ablav Ablxv (Very young to slightly developed, flat, medium to fine textured soils with seasonally high groundwater table) SLIGHTLY DEVELOPED, CRACKING CLAY SOILS, VERY POORLY DRAINED SLIGHTLY DEVELOPED, CRACKING CLAY SOILS, lmperfecty TO POORLY DRAINED Ablxa SLIGHTLY DEVELOPED, MODERATELY FINE TEXTURED SOILS, IMPERFECTLY DRAINED AbExa STRATIFIED, MEDIUM TEXTURED SOILS, IMPERFECTLY DRAINED AbEae STRATIFIED, MEDUM OVER MODERATELY FINE TEXTURED SOILS, POORLY DRAINED AbEa FINE TEXTURED SOILS, VERY POORLY DRAINED (WETLANDS) SOILS OF THE ALLUVIAL FANS FEx1 FEx2 (Gently undulating, very young to slighty developed soils with very deep groundwater table) GRAVELLY, COARSE TO MEDIUM TEXTURED SOILS, EXCESSIVELY DRAINED VERY GRAVELLY, LOAMY SOILS, EXCESSIVELY DRAINED Fix SLIGHTLY DEVELOPED, MODERATELY FINE TEXTURED SOILS, WELL DRAINED SOILS OF THE ESTUARINE PLAINS (Flat, very young to slightly developed soils with seasonally high groundwater table. The soils have commonly high E.SR and occasionally high ECe values) EEae STRATIFIED, MEDIUM TO FINE OVER COARSE TEXTURED SOILS, POORLY DRAINED EI/Exa ASSOCIATION OF VERY YOUNG (E) AND SLIGHTLY DEVELOPED (I), MODERÄELY FINE TEXTURED SOILS, POORLY DRAINED Soil phase: sodicity (and in places salinity) T«V««j Urban areas Railway., «._,.,, Border of study area km i

5 SOIL MAPOFNIKEA SCALE 1:10,000

6 LEGEND & / D/ NJ/R EA 1. SOILS OF THE TOPS OU km. 1 1 El VERY SHALLOW. VERY GRAVELLY. LOAMY SOILS /7 s / / 1Ip 1Ic3 (SANDY) CLAYLOAM SOILS, HAVING A SHALLOW PETROCALCIC HORIZON GRAVELLY, SANDY (CLAY)LOAM SOILS, HAVING A SHALLOW CALCIC HORIZON 4^ / % JW yy Si i \ 2Idj/ / ' I 3Vt s f Jr mt * J i5p 2Ic3 /y / ic^" 1\V \ \ 3Mv/c i\ 1 \ U! r^y \ J i \ \ / ' 1 /I '7/ (3Mv/<// Ic\! (21c3 \ Vu.\ V \\ \ \ v \\ \ \ VA \ V \ \ v\ \ \ \ \ V\\ \ V\ \ \WI \W \( v \\ k \ \ \ v\ \ \ A \ VA \\\\ \ V \\ \ \ \ \ 1Ic4 1I/E CLAY SOILS, HAVING A SHALLOW CALCIC HORIZON ASSOCIATION OFGRAVELLY SANDY (CLAY)LOAM SOILS. HAVING A SHALLOW CALCIC HORIZON. AND VERY SHALLOW, VERY GRAVELLY SOILS 2. SOILS OF THE SLOPES 2EI VERY SHALLOW, EXTREMELY GRAVELLY SOILS P2 Soil profile f / 1 fv^ L l bi/e^ slip Jl/E \ u 1 IV ƒ l \li/5/\ /3Mv/\ \ \ 2I/E 2Ic3 2Ic4 I 21/E VERY SHALLOW, GRAVELLY, SANDY (CLAY) LOAM SOILS, HAVING A CALCIC HORIZON WITHIN Wem FROM THE SURFACE VERY SHALLOW, CLAY SOILS, HAVING A CALCIC HORIZON WITHIN 40 cm FROM THE SURFACE ASSOCIATION OF GRAVELLY SOILS HAVING A SHALLOW CALCIC HORIZON. AND VERY SHALLOW, VERY GRAVELLY SOILS Ti2 Soil section (only chemical data available) Contour 2Id3 SOMEWHAT GRAVELLY, MODERATELY DEEP AND FINE TEXTURED SOILS ^szsss^' Streams 2Id4 MODERATELY DEEP, FINE TEXTURED SOILS 2Iv MODERATELY DEEP. CLAY SOILS HAVING VERTIC PROPERTIES Paved roads 2Mt MODERATELY DEEP, DARK, CLAY SOILS Unpaved roads 2flp SHALLOW, FINE TEXTURED SOILS, HAVING A PETROCALCIC HORIZON 2fI/E ASSOCIATION OF CLAY SOILS HAVING A CALCIC HORIZON, AND SHALLOW, VERY GRAVELLY, CLAYLOAMY SOILS N 3. SOILS OF THE VALLEY BOTTOMS 3Vt 3Mv STRONGLY SWELLING CLAY SOILS MODERATELY DEEP, DARK, CLAY SOILS, HAVING VERTIC PROPERTIES W 3Iv 3Mv/c CRACKING CLAY SOILS DEEP, DARK, CRACKING CLAY SOILS S 3E/M ASSOCIATION OF DARK, VERY SHALLOW AND GRAVELLY SOILS AND DARK, DEEPER. GRAVELLY, CLAY SOILS

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